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Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
The rise of calcifying nannoplankton in the Late Triassic (237–201 Ma) had profound consequences for the carbonate buffering capacity of the ocean. Research on the appearance of calcification typically focuses on the reasons that made this process
Externí odkaz:
https://doaj.org/article/64c1e6e9eb22462c9a6b9fe9534d8ff1
